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Structure of the Indian southwesterly pre-monsoon and monsoon boundary layers: Observations and numerical simulation

机译:印度西南季风前季风和季风边界层的结构:观测和数值模拟

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摘要

Characteristics of pre-monsoon and monsoon boundary layer structure and turbulence were studied in New Delhi and Bangalore, India during the summer of 1987. Micrometeorological towers were installed and instrumented at these locations to provide mean and turbulent surface layer measurements, while information on the vertical structure of the atmosphere was obtained using miniradiosondes. Thermal structures of the pre-monsoon and monsoon boundary layers were quite distinct. The daytime, pre-monsoon boundary layer observed over New Delhi was much deeper than that of the monsoon boundary layer observed over Bangalore and at times was characterized by multiple inversions. Surface, turbulent sensible heat fluxes at both sites were approximately the same (235 and 200 Wm−2 for New Delhi and Bangalore, respectively). Diurnal variations in the monsoon boundary layer at Bangalore were more regular compared to those under pre-monsoon conditions at New Delhi. One-dimensional numerical simulations of the pre-monsoon boundary layer using a turbulent energy closure scheme show good agreement with observations.
机译:1987年夏季,在印度新德里和班加罗尔研究了季风前和季风边界层结构和湍流的特征。在这些位置安装并安装了微气象塔,以提供均值和湍流表层测量,而垂直方向上的信息使用小型无线电探空仪获得大气的结构。季风前和季风边界层的热结构非常不同。白天,在新德里上空观测到的季风前边界层比在班加罗尔上空观测到的季风边界层要深得多,有时还具有多次反演的特征。两个地点的表面湍流显热通量大致相同(新德里和班加罗尔分别为235和200 Wm-2)。与新德里季风前条件相比,班加罗尔季风边界层的日变化更规律。利用湍流能量封闭方案对季风前边界层进行一维数值模拟,与观测结果吻合良好。

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